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Clastic sedimentary rock composed of at least 30 percent rounded to subangular fragments
larger than 2 mm in diameter; typically contains finer grained material in interstices
between larger fragments. If more than 15 percent of the fine grained matrix is of
indeterminant clastic or diagenetic origin and the fabric is matrix supported, may
also be categorized as wackestone. If rock has unsorted or poorly sorted texture with
a wide range of particle sizes, may also be categorized as diamictite.

note

Note this category is equivlanet to category labeled 'Conglomeratic rock in SLTTs
(2004), not to the category labeled 'Conglomerate' in that system.

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